Rainwater may play an important role in the process that triggers earthquakes, according to new research.
Researchers from the University of Southampton, GNS Science (New Zealand), the University of Otago, and GFZ Potsdam (Germany), identified the sources and fluxes of the geothermal fluids and mineral veins from the Southern Alps of New Zealand where the Pacific and Australian Plates collide along the Alpine Fault.
From careful chemical analyses, they discovered that fluids originating from the mantle, the layer below the Earth's crust, and fluids derived from rainwater, are channelled up the Alpine Fault.